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University of New Mexico

Relative Timing of Porphyroblast Growth and Peak Metamorphism in the Lower Granite Gorge, Grand Canyon, Arizona.

Abstract

dc:description.abstract

The Gneiss Canyon shear zone in the Lower Granite Gorge of the Grand Canyon represents an important Paleoproterozoic tectonic boundary between the Mojave and Yavapai provinces, and records west-side-up shear and NW-SE contraction at elevated temperature (~600 degrees Celsius). Movement took place on subvertical NE-striking foliation that forms the main tectonic fabric (S2). Travertine Canyon, east of the shear zone, preserves lower amphibolite grade Paleoproterozoic rocks with subvertical NE-trending fabric (S2). Prophyroblasts contain inclusion trails parallel to, and similar in morphology to, S2 indicating that porphyroblasts grew late or after S2 fabric development. Post-porphyroblast movements on S2 fabric involved rotation of porphyroblasts relative to matrix, shearing, and bending of S2 around porphyroblasts. Post-porphyroblast matrix coarsening indicates that metamorphism accompanied late adjustments on S2. Collectively, these data suggest that peak metamorphism occurred during the latest stages of NW-SE shortening on the previously formed S2 crenulation cleavage. In contrast, Spencer Canyon, west of the shear zone, preserves upper amphibolite grade rocks and porphyroblast textures that indicate peak metamorphism was synchronous with progressive deformation on northwest-trending fabrics. These NW fabrics are overprinted by the Gneiss Canyon shear zone at map scale and hence are at least in part older than S2. These fabrics and porphyroblasts are interpreted to record thrusting and decompression of high-grade upper plate rocks on the west side against colder lower plate rocks on the east side of the reverse sense Gneiss Canyon shear zone.

Degree

thesis:*
Name thesis:degree_name
Earth and Planetary Sciences
Level thesis:degree_level
Masters
Discipline thesis:degree_discipline
Department of Earth and Planetary Sciences
Year
1996

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Hutchison, Jimmie
Contributors dc:contributor
  • Karlstrom, Karl
  • Kudo, Albert M.

Subjects

dc:subject × 5

Rights

Language dc:language
English

Identifiers

dc:identifier.*
OAI identifier oai:identifier
oai:digitalrepository.unm.edu:eps_etds-1038

Chain of custody

source
Harvested from
University of New Mexico
Base URL
digitalrepository.unm.edu/do/oai/
Last updated
2026-07-24
Source record
OAI-PMH GetRecord
citation

Hutchison, Jimmie. Relative Timing of Porphyroblast Growth and Peak Metamorphism in the Lower Granite Gorge, Grand Canyon, Arizona.. Masters thesis, 1996. http://hdl.handle.net/1928/24717